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Rum
The mountainous, rugged island of Rum is the eroded remains of an early Tertiary volcanic
centre that existed at the time of the opening of the North Atlantic Ocean.
Many of the rocks found on Rum consist of layered ultramafic rocks
- remnants of the base of the volcano's magma chamber. It is not the only volcanic
centre on the west coast of Scotland to exhibit such layering, but the examples
seen on Rum are well exposed and in an excellent state of preservation. They
have become internationally important in their contribution to the understanding
of the origins of layering igneous intrusions. As with the other Scottish Tertiary
volcanic centres, Rum has been studied by many esteemed geologists such as
John Macculloch (1773 - 1835), John Wesley Judd (1879 - 1914) and Sir
Archibald Geikie, before being followed by more recent researchers such
as Dr Alfred Harker (1859 - 1939) and Sir Edward Bailey (1881 - 1965).

Askival and Hallival mountains of the Rum Cuillin.
Image provided
by Scottish Natural Heritage
The Rum Complex was intruded into Lewisian basement, Torridonian sandstones
(Precambrian), Mesozoic sedimentary rocks and early Tertiary lavas. The complex
itself evolved in two main stages. Initially, intrusive and extrusive activity
was charged by acid magmatism and associated with ring-faulting. It is thought
that the complex underwent repeated doming and subsidence (within the cauldron)
at this time. Rocks associated with this first phase include porphyritic felsite,
volcanic breccias and tuffs.

Askival and Hallival mountains of the Rum Cuillin.
Image provided
by Scottish Natural Heritage
The layered ultrabasic rocks were intruded during the second stage. The parent
magma is considered to be either high-temperature picritic basalt or feldspathic
peridotite that was subject to the right conditions that enabled it to rise
to within a short distance of the Earth's surface before crystallising. The
intrusions consist of sixteen layers of alternating feldspathic peridotite,
troctolite, troctolitic gabbro, feldspathic gabbro and anorthosite.
Note: The Rum volcanic centre forms part of the North Atlantic Tertiary Igneous
Province, along with the other centres of Skye, Arran, Ardnamurchan, Mull and
St. Kilda.
Further reading:
Craig, G.Y. 1991. Geology of Scotland. 3rd edn. The Geological Society, London.
Emeleus, C.H. & Gyopari, M.C. 1992. British Tertiary Volcanic Province,
Geological Conservation Review, Series No. 4. Joint Nature Conservation Committee,
Peterborough.
RUM NNR Website
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